Yardang Formation is a geomorphological process denoting the development of elongated, streamlined ridges through the preferential wind erosion of bedrock in arid environments, distinguished by its alignment with dominant paleowind directions and its occurrence in cohesive, fine-grained sediments.
24
Publications
1.4K
Citations
90
Authors
59
Institutions
Publications per year
2017–2026
8
Parents
Publications
24
1–5 of 24
Authors
90
- PK
4
h-index
- JD
3
h-index
- WL
2
h-index
- ZZ
2
h-index
- NC
2
h-index
1–5 of 90
Institutions
59
Chinese Academy of Sciences
Beijing, China
5 h-index
22 publications
1.1K citations
University of Arizona
Tucson, United States
4 h-index
7 publications
180 citations
Zhejiang University
Hangzhou, China
2 h-index
5 publications
155 citations
Planetary Science Institute
Tucson, United States
2 h-index
2 publications
191 citations
Nantes Université
Nantes, France
1 h-index
3 publications
87 citations
Southwest Research Institute
San Antonio, United States
1 h-index
1 publications
162 citations
Xinjiang Institute of Ecology and Geography
Ürümqi, China
1 h-index
2 publications
34 citations
Los Alamos National Laboratory
Los Alamos, United States
1 h-index
1 publications
29 citations
1–8 of 59
Venues
- Geomorphology
4 publications · 203 citations
4
h-index
- Journal of Geophysical Research Earth Surface
3 publications · 59 citations
3
h-index
- Aeolian Research
2 publications · 69 citations
2
h-index
- Journal of Geophysical Research Atmospheres
JGR · 2 publications · 360 citations
2
h-index
- Geological Society of America Bulletin
2 publications · 121 citations
2
h-index
1–5